Recent Landform Evolution (original) (raw)

In the Romanian Carpathians, developed on crystalline and volcanic rocks, the main geomorphological processes are rockfalls, debris fl ows, and topples. In the eastern part of the Eastern Carpathians, built up of Cretaceous and Paleogene fl ysch, landslides and mudfl ows are of major signifi cance. High and middle mountain karst features and cave systems are also widespread. In the alpine area of the Southern and Eastern Carpathians, avalanches are common on the steep slopes of

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